Manda-Inakir
Fissure vent · Ethiopia-Djibouti · 600m

- Type
- Fissure vent
- Country
- Ethiopia-Djibouti
- Region
- Eastern Africa / Afar Rift Volcanic Province
- Elevation
- 600m
- Coordinates
- 12.380, 42.200
- Last eruption
- 1928
- Tectonic setting
- Rift zone / Intermediate crust (15-25 km)
- Landform
- Cluster
- Major rock type
- Basalt / Picro-Basalt
Geological summary
Manda-Inakir consists of a series of NW-trending fissure vents and pyroclastic cones along the Ethiopia-Djibouti border. The elongated complex represents an uplifted mid-ocean ridge spreading center now exposed above sea level. An elongated dome of basement rocks is cut by two axial rifts, the northern of which was active during historical time. Basaltic cinder cones along the rift's marginal faults have produced lava flows on the flanks of the structural dome, yielding a shield-like morphology. An eruption in 1928 or 1929 at the SE end near the town of Korili (in Djibouti) produced the Kammourta cinder cone and a lava flow.
Eruption history
Summary (VEI over time)
Click a bar to see individual eruptions
Detailed timeline
- 1928VEI 2Observed1928-12-31 – OngoingKammourta
External links
⚠ For reference only. Not for emergency response.